activity 4 locating an earthquake epicenter answer key

4. The Richter scale was created in the 1930s to assign a single number to quantify the energy released during earthquakes. Click on New Document and select the file importing option: upload Locating the epicenter of an earthquake worksheet answer key from your device, the cloud, or a protected link. Focus (aka Hypocenter) is the location in the Earth where the earthquake starts. "`B(R6sj [CX7p+s =#;~ `'kA xb``d``Id`a`Ab@_ :iWGi>|q` 0000010002 00000 n Fill Locating The Epicenter Of An Earthquake Worksheet Answers, Edit online. 9 - Legal. The lag time for any pen recorded the arrival of P, S, and surface A circle is drawn from each of the three different seismograph locations, where the radius of each circle is equal to the distance from that station to the epicenter. =Cv :~4yrXP 62{_,*Uq/O-oUNBr-$y~:G},#3e^CS6U*_zVGY7ZNUWk2f?? {%!,"{u5E&OOqA_"/uxn-kx+Vz*EQb)Q We additionally manage to pay for . Conclude the activity with a class discussion (and perhaps homework questions) to share ideas and answers, as described in the Assessment section. important in helping seismologists determine the epicenter of the earthquake. Scientists use triangulation to find the epicenter of an earthquake. A minimum of three seismic stations is necessary to locate an epicenter. Facility Name Busine Child ren Information Child Name C. Child Social Security Number Type of Case being filed - Check only one category. The spot where those three circles intersect is the epicenter (Figure 13.12). Using 3 seismograms the students will be able to triangulate the epicenter of an earthquake. A circle with a radius of the distance to the quake can be drawn. The American Geosciences Institute represents and serves the geoscience community by providing collaborative leadership and information to connect Earth, science, and people. 0000079769 00000 n How do we determine the epicenter of an earthquake? P and S arrivals, you can now locate an earthquake your answers below. Analyze and interpret data on natural hazards to forecast future catastrophic events and inform the development of technologies to mitigate their effects. minutes and P waves 8 minutes to So the difference in the P- and S-wave arrival times determines the distance between the epicenter and a seismometer. To make a magnitude determination, two measurements are needed: the S-P interval (already determined earlier in the tutorial) and the maximum amplitude of the seismic waves. This opens a new window to Michigan Techs UPSeis informational site about earthquakes and seismology. Richter magnitude scale: An earthquake measurement scale created in the 1930s to assign a single number to quantify the energy released during earthquakes. Moment magnitude scale. 92 0 obj <>/Filter/FlateDecode/ID[]/Index[83 25]/Info 82 0 R/Length 62/Prev 466624/Root 84 0 R/Size 108/Type/XRef/W[1 2 1]>>stream This is determined by the P-and S-wave arrival times. Three seismographs are needed. 0000006538 00000 n distance = travel time for S waves earthquakes. travel 3,000 miles. 100 km 4.1 km/s 24.4 s; Finding the epicenter (continued) data table analyze and conclude answer the following questions on a separate sheet of paper. Before looking at the Earthquakes Living Lab, have pairs complete the, Then guide the teams to the Earthquakes Living Lab via the living lab website at. The point where your ruler crosses the middle line on the chart marks the magnitude (strength) of the earthquake. Thus technology use varies from region to region and over time. 0 Earthquakes & Volcanoes Test Review Answers. Locating An Earthquake Epicenter Lab Answers Thank you for reading Locating An Earthquake Epicenter Lab Answers . *The NGSS logo is a registered trademark of WestEd. Subject Areas: A circle is drawn from each of the three different seismograph locations, where the radius of each circle is equal to the distance from that station to the epicenter. What did it feel like? 0000002544 00000 n Accessibility StatementFor more information contact us atinfo@libretexts.orgor check out our status page at https://status.libretexts.org. Then locate and click the link in the center of the page under the question: "How is an earthquake epicenter located and how is magnitude determined?" 4. Students first triangulate the location of an earthquake's epicenter, then calculate its magnitude. Divide the class into student pairs, and have them assemble at their computers with journals/paper and writing instruments. !D,X2:azTG)kPT~Mj 4>d w@O'. Locating Earthquake Epicenter Lab Answer Key buysms de. Do you agree with this alignment? hWmo9+[+UH EkNB|6YiaVJ=cRh7{T1R,5LI1$K=s)XR&87@&$LTPLutlcyNuzjf--\?qaXZM&HM.Eg"HnTqSWqN0&~2kf0 Md|d&:zhe)7I? Locating Earthquake Epicenter Lab - Triangulation sheet for students and/or teachers to use (Slide 6), and answer key (Slide 7). long will it take, to the nearest 0. minutes, for the first P waves to travel from the epicenter to your station? waves from a distant earthquake. Video Guide / Worksheets and Quizzes for Quizzes and Answer Sheet __ 2. The magnitude determination is based on seismic data. I contacted the persons listed below to find out the location of the following people entitled to notice Name of Person Measure the difference in arrival times between the first shear (s) wave and the first compressional (p) wave, which can be interpreted from the seismogram. A.45 seconds B.50 seconds C.55 seconds D.65 seconds Answer Key: D The farther away the epicenter is, the greater the difference . The instrument detects and documents the intensity, direction and duration of ground vibrations, which are used to determine the epicenters and strength/magnitudes of earthquakes or other seismic events. located 1,000 miles from the lag time. Triangulation is required to determine exactly where it happened. Review their answers to assess their base knowledge of the subject matter. 0000002383 00000 n 3000 miles. and S waves depends on the distance from the epicenter of the answer the following question. 0000004224 00000 n Must engineers be content with mitigating disasters, instead of preventing them? 74 Earthquake Activity: Locating the Epicenter and Time of Earthquake . longer or shorter). Triangulation and Magnitude: Student pairs complete the worksheet, which includes following a tutorial/simulation accessed through the Earthquakes Living Lab. Direct student pairs to independently complete the tutorial/simulation to find an epicenter location via the triangulation method and compute the earthquake magnitude: The simulation directs students to look at three simplified seismograms from seismic stations in Chile (Talca, Santiago, Osorno) and select the correct measurements of the S-P intervals. Accessed December 11, 2013. http://en.wikipedia.org/wiki/Moment_magnitude_scale, Novak, Gary. seismogram. Success is figuring out that the epicenter is just off the coast of Chile, where the three circles intersect. S-P interval: The time interval between the arrivals of P and S waves. Specifically, seismographs make recordings (seismograms) of the seismic waves generated from earthquakes, providing engineers and other researchers with data that they use to make predictions about future earthquakes. The hypocenter is the point within the earth where an earthquake rupture starts. Please answer the following questions using the earthquake video shake, shake, shake. 0000000956 00000 n All rights reserved. Yw8SxGk}X3kfTfW& gk`41#'uf7"G\fsN4^8jC7[+%`qFLFKpFc 0000006984 00000 n At least 3 earthquake recording stations are required to find the location of the earthquake epicenter. As you may know, people have look numerous times for . In Figure 13.9, there is an example seismogram from a station that includes a minor earthquake. Before going to the classroom, you will need to: Provide each student, with the following: Earthquakes occur every day all over the United States and all over the world. Type text, add images, blackout confidential details, add comments, highlights and more. To complete the activity, some prior . Lab Exercise #2: Locating the Epicenter of an Earthquake In this lab exercise, you will locate the epicenter of an earthquake. El trmino tambin puede hacer referencia al ttulo o nombre de alguien a quien se di, Practica II - De Psicologian membrete es aquello que se ubica en el sector superior de una pgina, mencionando el ttulo o el nombre de un individuo, una empresa, etc. Introduction: Before student pairs look at the Earthquakes Living Lab, direct them to complete the Engage section of the Finding Epicenters and Measuring Magnitudes Worksheet, which asks them to apply any prior knowledge and/or speculate as to what the Richter magnitude scale is and what an epicenter is. How might they use this information? Activity 4 Locating An Earthquake Epicenter Answers: Fill Out & Sign . It travels faster than the same earthquake's S wave (almost double the speed) and is similar to sound waves. Activity 4: Locating an Earthquake Epicenter Examining Seismograms The three basic types of seismic wave generated by an earthquake at its focus are Pwaves, Swaves, and Surface waves. Last updated November 26, 2013. The spot where those three circles intersect is the epicenter (Figure 13.12). How does distance from the epicenter affect the S-P time interval? Figure 1 is a simplified example of a Answer Key: Lab 5 Earthquakes - Find People EARTHQUAKES: Epicenter Determination and Seismic Waves . The magnitude is the logarithm of the amplitude of the ground wave. consider a seismograph stationed 3, Civil engineers, who design houses, apartment buildings, schools, skyscrapers, bridges, highways, tunnels, water treatment facilities, factories and other structures, may use this data to help them create safer structures that are less likely to sustain damage during earthquakes. (Grades 9 - 12). There are two sets of data and maps to do this activity/ lab for than once. 0000006011 00000 n Alignment agreement: Locating the epicenter of an earthquake worksheet answer key, locating the epicenter of an earthquake worksheet pdf, chapter 7 lab 1 locating epicenters answer key, how many seismographs are needed to locate the epicenter of an earthquake. 107 0 obj <>stream Using the real-world data in the living lab enables students and teachers to practice analyzing data to solve problems and answer questions, in much the same way that scientists and engineers do every day. 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This worksheet focuses on using the p and s graph to find different variables. The nations most famous fault is the San Andreas Fault, which runs along a north-south trend in southern California, and happens to run directly through Los Angeles. Students learn about factors that engineers take into consideration when designing buildings for earthquake-prone regions. time for any point that is 3,000 miles Do you agree with this alignment? The vertical lines, spaced one, minute apart, represent the passage of time, (from left to right). ' endstream endobj 69 0 obj <> endobj 70 0 obj [85 0 R] endobj 71 0 obj <> endobj 72 0 obj <> endobj 73 0 obj <>stream 83 0 obj <> endobj 0000000856 00000 n As the drum rotated, t, pen recorded the arrival of P, S, and surface, between arrival of P and S waves is called, epicenter, the longer the lag time measured, velocity, amplitude, and frequency of the. Describe the logarithmic nature of the earthquake magnitude scale. During an earthquake, seismic waves are sent all over the globe. 0000003254 00000 n Several thousand seismographs exist at locations around the planet, continuously measuring abnormalities in the Earth's movement. Get the inside scoop on all things TeachEngineering such as new site features, curriculum updates, video releases, and more by signing up for our newsletter! Locating an Epicenter through Triangulation of Seismic Data- Remote/Hybrid/Live. Resources. All 100,000+ K-12 STEM standards covered in TeachEngineering are collected, maintained and packaged by the Achievement Standards Network (ASN), Looking at the nomogram, students click on each location data point to see where the three lines intersect to read the estimated magnitude. 1. The earthquake occurred somewhere along that circle. 4. fault - a fracture in Earth's crust where the rocks on either side have moved. 17 Station St., Ste 3 Brookline, MA 02445. endstream endobj 84 0 obj <> endobj 85 0 obj <> endobj 86 0 obj <>stream In order to determine the location of an earthquake epicenter, seismographs from at least three different places are needed for a particular event. If a quake is far from the seismograph, the P-waves arrive long before the S-waves. A. Seismic waves-waves generated by an earthquake, can move the ground forward and back- answers the question. If the lag time were measured at a location closer to the epicenter, The period of a wave is the time between two adj, How does the period of the P waves compare to t. Use data from seismograms to locate the epicenters of earthquakes. 01. This activity is designed around the Earthquakes Living Lab, a resource and online interface that uses real-time U.S. Geological Survey seismic data from around the world. Epicenter is the location on the surface of the Earth directly above where the earthquake starts. Swaves arrive at the seismic station after the Pwaves. To locate the epicenter of the earthquake, seismologists use the . HTAn Q(_?!6YV3B"\'9:4gTp*7^/P.X!skfkJ)1nG#a\{UD+iWM+ rQR]9SFTUPlM#"c:;tnsQPlu]Uyv?Ge}W;8cMA/x}'5clES~+}S+N7}wQ:/BkmI^" 5oqaBC[TRjq4.e}F:SQg{=u\xcg~EaZKReoC?oahJ` 'w endstream endobj 77 0 obj <>stream farther from the epicenter of an earthquake? They use three seismographs in a process called triangulation to determine earthquake epicenters. Subjects: Earth Sciences, General Science Grades: 5th - 8th Types: Activities, Laboratory seismograph: An instrument that measures motions of the ground, including those of seismic waves generated by earthquakes. 0000001861 00000 n activity illustrates how the epicenter of an earthquake is found. HTn {0,`K6}(J6]&Q^"!q57y_VQ9fp3/?Mc=KGsrrt:c\$Lh`4}>C>`qcSj0[YpZ_Su(322/N Z./$E )H %C[5ph[BUyGh7|!XPQiDjJ(|BNvylk+g;9G(#Aby>Jcf`XmnwtDD+;Z^I&Sb-4!7oi` L7 endstream endobj 78 0 obj <> endobj 79 0 obj <>stream /g$=#!$EbBbhD!,x so^6Uc})\uJs=fyY}j'|YjTm8B_[}*Ovm\[J'.mu?lQg,wzJM^X&P w>-T%*h%J4 yB@VPmP]@D------------,2dfY$"A!ANAASi)4$dniiiinH% Gxt5DJ) )9RRr$II'y ??O's^3@[{*{VT?nsNS!ilq]mFO?? Considered best for measuring small earthquakes (3.5 M or less). Sharing Information/Thinking Ahead: In the Evaluate section of the worksheet, student pairs are asked to compose answers to two questionswhether they think seismology is a reliable science and ways seismic data is useful for engineers. The uses of technologies and any limitations on their use are driven by individual or societal needs, desires, and values; by the findings of scientific research; and by differences in such factors as climate, natural resources, and economic conditions. When seismic data is collected from at least three different locations, it can be used to determine the epicenter by where it intersects. 1. If a quake is far from the seismograph, the P-waves arrive long before the S-waves. THREE SEISMOGRAMS Seismogram A - New York, NY 1 minute 1. The USGS Earthquake Hazards Program is part of the National Earthquake Hazards Reduction Program (NEHRP), established by Congress in 1977, and the USGS Advanced National Seismic System (ANSS) was established by Congress as a NEHRP facility. Assess their understanding based on the thoroughness of their answers. HtA1D41`s(GME$Ke*YdEOYf2-:r. Finally, the location of the 3 seismographs are placed on a map and the distance to the epicenter is used to draw a circle with an origin at each seismograph and a radius equal to the distance to the epicenter as taken from each seismogram. Every earthquake is recorded on numerous seismographs located in different directions. Engineers first determine where earthquakes are likely to occur, and how severe they are likely to be. Tracings made at three separate seismic stations are needed to locate an earthquake epicenter. All the arcs should intersect at a common point - the epicenter. S wave: The second seismic wave of an earthquake. Students also investigate which structural designs are most likely to survive an earthquake. [N'. [*aiLG?+J\QI86~}ooRrr!pm}dk@dBbZPMZlC4C\9^ SM.R\!H+$|+DUzt^w{" %&{KXjT'9yzT^UFe:+f(`PU_9%EW@\)?i qp!\G Z endstream endobj 75 0 obj <>stream d>(ZvO= hbb2b`b``a I @ endstream endobj 62 0 obj <>/Metadata 55 0 R/Pages 51 0 R/StructTreeRoot 57 0 R/Type/Catalog/ViewerPreferences<>>> endobj 63 0 obj <>/Font<>>>/Fields[]>> endobj 64 0 obj <>/Font<>/ProcSet[/PDF/Text]>>/Rotate 0/TrimBox[0.0 0.0 612.0 792.0]/Type/Page>> endobj 65 0 obj <> endobj 66 0 obj <> endobj 67 0 obj <> endobj 68 0 obj <>stream (5 minutes) Discuss how gathering information on epicenters can be applied. 5 4. 0000005149 00000 n ACTIVITY 4.2B Locating an Earthquake Figure 4.5 shows seismograms for the same earthquake recorded at three locations - New York, Nome, Alaska, and Mexico City. hb```f``Rl@ (l"`+uk?0.a~@6Vm;| G3f`75@v@Wz|A4#w9{(` ) Another method of locating an earthquake is to use the P-wave arrival-time minus origin-time (P - O) interval instead of distance. Finding the epicenter of an Earthquake by Ah - Ha Lessons 5.0 (1) $3.00 PDF Activity This lesson teaches the student the process scientists use to locate the epicenter of an EQ. Use Figure 4.5 and the travel-time graph in Figure 4.4 to determine the distance between each station and THREE SEISMOGRAMS the epicenter. Answer the following questions in the spaces provided. How many minutes elapsed between the arrival of the first P wave and the last measurable They make a model of a seismographa measuring device that records an earthquake on a seismogram. Locating the Epicenter of an Earthquake - SE Asia a foldable activity, slide presentation to guide reading, and an answer key! (Source: USGS, Wikipedia). Figure 2. 0000030968 00000 n How does the period of the P waves compare to the period of the surface waves? Then from the same recordings they determine the earthquake's magnitude, an estimate of the amount of energy released during the earthquake. If you can't find an answer to your question, please contact us. Once three seismographs have been located, find the time interval between the arrival of the P-wave . Student exploration Graphing Skills SE Key Gizmos Explore Learning. 0000106240 00000 n What was the lag time (in minutes) at this location? Multiply the difference by 8.4 to estimate the distance, in kilometers, from the seismograph station to the epicenter. Last modified July 18, 2012. It's a logarithmic scale from 1 to 10 with each succeeding level representing 10 times as much energy as the last. Wikipedia, The Free Encyclopedia. graph. For example, This is determined by the P-and S-wave arrival times. How does the Mad Scientist. (Grades Take a few minutes to read the information on the left side of this page for the 2010 earthquake off the coast of central Chile. Many updates and improvements! 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